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Copper Basin (Tennessee)

Geological area in southeastern Tennessee, United States

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Through Copper, American Civil War and Sulfur

Copper was first discovered in the basin in 1843, and by the 1850s large mining operations, spearheaded by German-born businessman Julius Eckhardt Raht, were taking place. The mines were seized by the Confederacy during the American Civil War and were the source of about 90% of the copper used by the Confederate Army. After the Civil War, smelting operations, which were used to separate sulfur from the copper ore, resulted in acid rain in the area. Combined with the logging of nearby forests to fuel the smelters, this resulted in a massive environmental disaster that left the surrounding landscape barren for more than a century. Several mines, the largest of which was the Burra Burra Mine, operated in the basin.

By the 1950s, mining operations in the Copper Basin began to decline, with the final mine closing in 1987. Today, the Ducktown Basin Museum chronicles the geological record and history of the mining operations in the basin.

Geography and geology

The Copper Basin is located in a broad valley in the Blue Ridge Mountains, part of the southern Appalachian Mountains near the borders of Tennessee, North Carolina, and Georgia. The basin, actually an area of low hills rather than a true basin, is surrounded on all sides by mountains, including Pack Mountain to the east, Stansbury Mountain to the north, Little Frog Mountain to the northwest, and Big Frog Mountain to the southwest, some more than 4,000 feet (1,200 m) above sea level. A series of hills rise above the basin to the south. The basin has an average elevation of 1,650 feet (500 m) above sea level.

The Ocoee River flows through the southwestern section of the Copper Basin, entering from Georgia, where it is known as the Toccoa, and exiting via a scenic gorge between Big Frog Mountain and Little Frog Mountain to the west. The river's Copper Basin segment is located at just over 35 miles (56 km) upstream from the river's mouth along the Hiwassee River near Benton, Tennessee. The Tennessee Valley Authority's Ocoee Dam Number 3 created a reservoir that extends into the Copper Basin.

Ducktown is located in the center of the Copper Basin near the juncture of Tennessee State Route 68 and U.S. Route 64. The city of Copperhill is located on the southern portion of the basin near the Tennessee-Georgia border and directly borders McCaysville, Georgia. Other communities include Postelle in the northwest section of the basin, Isabella in the eastern portion, and Harbuck, Turtletown, and Farner just north of the basin. The Copper Basin is also included in the Cleveland, Tennessee, metropolitan area.

Most of the rocks in the Copper Basin are metamorphic rocks deposited during the Lower Cambrian period but also include some igneous rocks. The metamorphic rocks are part of the Great Smoky formation. About two thirds of this metamorphic rock is greywacke, and it is also made up of arkose, conglomerate, greywacke conglomerate, schist, mica schist, garnet schist, slate, and staurolite. The igneous rock consists predominantly of gabbro. The first copper ores were deposited during the Ordovician period, when igneous rocks were advancing into the area. During this time, limestone in the area was metamorphosed into marble. Additional ore was formed after the end of the Carboniferous period. The rocks in the Copper Basin are some of the oldest rocks that were deposited during the Paleozoic era. The copper is located in three paralleling veins within the basin.

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